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Kyanite-rich and quartz-rich eclogites occur as lenses within amphibolite-facies quartzo-feldspathic gneisses in the Pohorje Mountains, Northern Slovenia, that form the easternmost Austroalpine basement. Major and trace elements indicate that the kyanite-rich eclogites were derived from plagioclase-rich gabbroic cumulates, whereas the quartz-rich eclogites represent more fractionated basaltic compositions...
The precise timing of metasomatic events in the Kaapvaal craton lithospheric mantle is poorly constrained and therefore it has proven difficult to relate mantle metasomatism in the source to igneous activity at the surface. A suite of mica-amphibole-rutile-ilmenite-diopside-bearing xenoliths (MARID) represents the product of such metasomatic fluids or melts. In this paper we report results of a SHRIMP...
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